A C-NMR study on the influxes into the tricarboxylic acid cycle of a renal epithelial cell line, LLC-PK1/Cl4: the metabolism of [2-C]glycine, l-[3-C]alanine and l-[3-C]aspartic acid in renal epithelial cells

Perchloric acid extracts of LLC-PK₁/Cl₄ cells, a renal epithelial cell line, incubated with either [2-¹³C]glycine l-[3-¹³C]alanine, or d,l-[3-¹³C]aspartic acid were investigated by ¹³C-NMR spectroscopy. All amino acids, except labelled glycine, gave rise to glycolytic products and tricarboxylic acid cycle (TCA) intermediates. For the first time we also observed activity of γ-glutamyltransferase activity and glutathione synthetase activity in LLC-PK₁ cells, as is evident from enrichment of reduced glutathione. Time courseS showed that only 6% of the labelled glycine was utilized in 30 min, whereas 31% of l-alanine and 60% of l-aspartic acid was utilized during the same period. ¹³C-NMR was also shown to be a useful tool for the determination of amino acid uptake in LLC-PK₁ cells. These uptake experiments indicated that glycine alanine and aspartic acid are transported into Cl₄ cells via a sodium-dependent process. From the relative enrichment of the glutamate carbons, we calculated the activity of pyruvate dehydrogenase to be about 61% of when labelled l-alanine was the only carbon source for LLC-PK₁/Cl₄ cells. Experiments with labelled d,l-aspartic, however, showed that about 40% of C-3-enriched oxaloacetate (arising from a de-amination of aspartic acid) reached the pyruvate pool.     

The dynamics of neutral sugars in the rhizosphere of wheat. An approach by13C pulse-labelling and GC/C/IRMS

Rhizodeposition, i.e. the release of carbon into the soil by growing roots, is an important part of the terrestrial carbon cycle. However thein situ nature and dynamics of root-derived carbon in the soil are still poorly understood. Here we made an investigation of the latter in laboratory experiments using¹³CO₂ pulse chase labelling of wheat (Triticum aestivum L.). We analyzed the kinetics of¹³C-labelled carbon and more specially¹³C carbohydrates in the rhizosphere. Wheat seedlings-soil mesocosms were exposed to¹³CO₂ for 5 hours in controlled chambers and sampled repeatedly during two weeks for¹³C/C analysis of organic carbon. After a two-step separation of the soil from the roots, the amount of total organic¹³C was determined by isotope ratio mass spectrometry as well as the amounts of¹³C in arabinose, fructose, fucose, glucose, galactose, mannose, rhamnose and xylose. The amount and isotopic ratio of monosaccharides were obtained by capillary gas chromatography coupled with isotope ratio mass spectrometry (GC/C/IRMS) after trimethyl-silyl derivatization. Two fractions were analyzed : total (hydrolysable) and soluble monomeric (water extractable) soil sugars. The amount of organic¹³C found in the soil, expressed as a percentage of the total photosynthetically fixed¹³C at the end of the labelling period, reached 16% in the day following labelling and stabilised at 9% after one week. We concluded that glucose under the form of polymers was the dominant moietie of rhizodeposits. Soluble glucose and fructose were also present. But after 2 days, these soluble sugars had disappeared. Forty percent of the root-derived carbon was in the form of neutral sugars, and exhibited a time-increasing signature of microbial sugars. The composition of rhizospheric sugars rapidly tended towards that of bulk soil organic matter.     

Pulse-labelling a cover crop with 13C to follow its decomposition in soil under field conditions

A preliminary study was conducted using the stable isotope ¹³C to pulse label the cover crop phacelia (Phacelia tanacetifolia) to examine its decomposition in soil, under field conditions. Plants were grown, in pots, in the greenhouse and after four weeks of growth were labelled with ¹³CO₂ six times, at 1–2 week intervals. A single chamber was placed over the pots, and ¹³CO₂ was generated, inside the chamber, by injecting lactic acid into sodium carbonate (99 atom % ¹³C). For calculating the quantity of Na₂CO₃ required, a target enrichment of 5 atom% ¹³C within the shoots of plants, assuming no respiration losses, was used. When harvested, at flowering, the mean enrichment of the shoot material was 3.0466 atom% ¹³C, or 1.9654 atom% excess ¹³C. To assess uniformity of labelling within plants, the shoot of a single plant was divided into leaves and stem from three sections of equal length. Ninety-three percent of this plant's dry matter had a ¹³C enrichment within 20 % of the weighted mean. At a field site with sandy soil, ¹³C labelled shoot and root material were combined and mixed with soil (0–15 cm). The soil was sampled 16 and 179 days later to determine the recovery of the added excess ¹³C in soil total C. The recoveries in soil (0–30 cm) were, respectively, 78 and 40 % at 16 and 179 days; there was appreciable variation associated with the recovery data from day 16, much less so at day 179. Methodological procedures for (i) enhancing the uniformity of labelling with ¹³C within plants, and (ii) minimising variability in the recovery of ¹³C from soil are suggested. ei]R Merckx     

Incomplete 13C labelling of α-pinene content of Quercus ilex leaves and appearance of unlabelled C in α-pinene emission in the dark

α ‐Pinene is formed in and emitted by Quercus ilex leaves. The carbon emitted as α ‐pinene is rapidly and totally labelled by ¹³C in CO₂ in air, but α ‐pinene contained in the leaf shows a fraction of completely unlabelled carbon even after long exposures to air containing only ¹³CO₂. When the labelled leaf is darkened, α ‐pinene emission drops but is still measurable for about 10 h, and carbon becomes partially unlabelled. After an 11 h darkening the α ‐pinene content is still as high as in the light but the carbon is mostly unlabelled. If the leaf is re‐illuminated but photosynthesis is inhibited by removing CO₂ and lowering O₂, a burst of emission occurs and the content of α ‐pinene is depleted. Our experiments suggest that a pool of α ‐pinene which is not directly generated by photosynthesis intermediates exists. Since this pool does not contribute relevantly to the emission in the light, we hypothesize that it is inhibited in the light and spatially located in a different compartment from chloroplasts. As we discuss, glycolysis in the cytoplasm and leucine catabolism in the mitochondria are both possible extra‐chloroplasts sources of carbon for isoprenoids.     

Photosynthesis and apparent affinity for dissolved inorganic carbon by cells and chloroplasts of Chlamydomonas reinhardtii grown at high and low CO2 concentrations

Chloroplasts with high rates of photosynthetic O₂ evolution (up to 120 mol O₂· (mg Chl)^-1·h^-1 compared with 130 mol O₂· (mg Chl)^-1·h^-1 of whole cells) were isolated from Chlamydomonas reinhardtii cells grown in high and low CO₂ concentrations using autolysine-digitonin treatment. At 25° C and pH=7.8, no O₂ uptake could be observed in the dark by high- and low-CO₂ adapted chloroplasts. Light saturation of photosynthetic net oxygen evolution was reached at 800 mol photons·m^-2·s^-1 for high- and low-CO₂ adapted chloroplasts, a value which was almost identical to that observed for whole cells. Dissolved inorganic carbon (DIC) saturation of photosynthesis was reached between 200–300 M for low-CO₂ adapted chloroplasts, whereas high-CO₂ adapted chloroplasts were not saturated even at 700 M DIC. The concentrations of DIC required to reach half-saturated rates of net O₂ evolution (K_m(DIC)) was 31.1 and 156 M DIC for low- and high-CO₂ adapted chloroplasts, respectively. These results demonstrate that the CO₂ concentration provided during growth influenced the photosynthetic characteristics at the whole cell as well as at the chloroplast level.Abbreviations Chl chlorophyll - DIC dissolved inorganic carbon - K_m(DIC) coneentration of dissolved inorganic carbon required for the rate of half maximal net O₂ evolution - PFR photon fluence rate - SPGM silicasol-PVP-gradient medium     

Polyglucose synthesis in Chloroflexus aurantiacus studied by 13C-NMR

Chloroflexus aurantiacus OK-70 fl was grown photoautotrophically with hydrogen as electron source. The cultures were subjected to long term labelling experments with ¹³C-labelled acetate or alanine in the presence of sodium fluoroacetate. The presence of fluoroacetate caused the cells to accumulate large amounts of polyglucose which was hydrolysed and analysed by NMR. The labelling patterns of glucose were symmetric and in agreement with carbohydrate synthesis from acetate and CO₂ via pyruvate synthase. The content of carbon derived from added acetate was highest in C2 and C5 of glucose, at least 20% higher than in C1 and C6. About one third of the glucose carbon was derived from added acetate, the rest being from CO₂. Contrary to expectations, in glucose formed in the presence of C1-labelled acetate C1 and C6 contained more label than C2 and C5, and with C2-labelled acetate as the tracer glucose was mainly labelled in C2 and C5. Labelled CO₂ was formed from acetate labelled at either position. The labelling data indicate a new metabolic pathway in C. aurantiacus. It is suggested that the cells form C1-labelled acetyl-CoA from C2-labelled acetyl-CoA and vice versa by a cyclic mechanism involving concomitant CO₂ fixation and that this cycle is the part of the autotrophic CO₂ fixation pathways in C. aurantiacus in which acetyl-CoA is formed from CO₂.The polyglucose of C. aurantiacus appears to have predominantly (1–4)-linked structure with about 10% (1–6)-linkages as revealed by ¹³C-NMR.     

Water status related photosynthesis and carbon isotope discrimination in species of the lichen genusPseudocyphellaria with green or blue-green photobionts and in photosymbiodemes

Summary Green lichens have been shown to attain positive net photosynthesis in the presence of water vapour while blue-green lichens require liquid water (Lange et al. 1986). This behaviour is confirmed not only for species with differing photobionts in the genusPseudocyphellaria but for green and blue-green photobionts in a single joined thallus (photosymbiodeme), with a single mycobiont, and also when adjacent as co-primary photobionts. The different response is therefore a property of the photobiont. The results are consistent with published photosynthesis/water content response curves. The minimum thallus water content for positive net photosynthesis appears to be much lower in green lichens (15% to 30%, related to dry weight) compared to blue-greens (85% to 100%). Since both types of lichen rehydrate to about 50% water content by water vapour uptake only green lichens will show positive net photosynthesis. It is proposed that the presence of sugar alcohols in green algae allow them to retain a liquid pool (concentrated solution) in their chloroplasts at low water potentials and even to reform it by water vapour uptake after being dried. The previously shown difference in δ¹³C values between blue-green and green lichens is also retained in a photosymbiodeme and must be photobiont determined. The wide range of δ¹³C values in lichens can be explained by a C₃ carboxylation system and the various effects of different limiting processes for photosynthetic CO₂ fixation. If carboxylation is rate limiting, there will be a strong discrimination of¹³CO₂, at high internal CO₂ partial pressure. The resulting very low δ¹³C values (-31 to-35‰) have been found only in green lichens which are able to photosynthesize at low thallus water content by equilibraiton with water vapour. When the liquid phase diffusion of CO₂ becomes more and more rate limiting and the internal CO₂ pressure decreases, the¹³C content of the photosynthates increases and less negative δ¹³C values results, as are found for blue-green lichens.     

C-nuclear magnetic resonance studies of the biosynthesis of 5-aminolevulinic acid destined for chlorophyll formation in dark-grown Scenedesmus obliquus

The ¹³C-nuclear magnetic resonance (NMR) spectra of chlorophyll a formed in dark-grown Scenedesmus obliquus (Turp.) Kützing in the presence of [1-¹³C]glutamate, [2-¹³C]- and [1-¹³C]glycineshowed that the ¹³C of glutamate was specifically incorporated into the eight-carbon atoms in the tetrapyrrole macrocycles derived from C-5 of 5-aminolevulinic acid (ALA), while the C-2 of glycine was only incorporated into the methyl carbon of the methoxycarbonyl group attached to the isocyclic ring of chlorophyll a. No specific enrichment of these nine carbon atoms was observed in the spectrum of chlorophyll a formed in the presence of [1-¹³C]-glycine. These labeling patterns provide evidence for the operation of the C₅-pathway and against the operation of the ALA synthase pathway for chlorophyll formation in darkness.     

Simultaneous CT-13C and VT-15N chemical shift labelling: Application to 3D NOESY-CH3NH and 3D 13C,15N HSQC-NOESY-CH3NH

Based on the HSQC scheme, we have designed a 2D heterocorrelated experiment which combines constant time (CT) ¹³C and variable time (VT) ¹⁵N chemical shift labelling. Although applicable to all carbons, this mode is particularly suitable for simultaneous recording of methyl-carbon and nitrogen chemical shifts at high digital resolution. The methyl carbon magnetisation is in the transverse plane during the whole CT period (1/J_CC=28.6 ms). The magnetisation originating from NH protons is initially stored in the 2H_zN_z state, then prior to the VT chemical shift labelling period is converted into 2H_zN_y coherence. The VT -¹⁵N mode eliminates the effect of ¹ J _N,CO and ^1,2 J _N,CA coupling constants without the need for band-selective carbon pulses. An optional editing procedure is incorporated which eliminates signals from CH₂ groups, thus removing any potential overlap with the CH₃ signals. The CT-¹³CH₃,VT-¹⁵N HSQC building block is used to construct two 3D experiments: 3D NOESY-CH₃NH and 3D ¹³C,¹⁵N HSQC-NOESY-CH₃NH. Combined use of these experiments yields proton and heteronuclear chemical shifts for moieties experiencing NOEs with CH₃ and NH protons. These NOE interactions are resolved as a consequence of the high digital resolution in the carbon and nitrogen chemical shifts of CH₃ and NH groups, respectively. The techniques are illustrated using a double labelled sample of the CH domain from calponin.     

Biosynthesis of artemisinin – revisited

Artemisinin is a well-known antimalarial drug isolated from the Artemisia annua plant. The biosynthesis of this well-known molecule has been reinvestigated by using [1-¹³C]acetate, [2-¹³C]acetate, and [1,6-¹³C₂]glucose. The ¹³C peak enrichment in artemisinin was observed in six and nine carbon atoms from [1-¹³C]acetate and [2-¹³C]acetate, respectively. The ¹³C NMR spectra of ¹³C-enriched artemisinin suggested that the mevalonic acid (MVA) pathway is the predominant route to biosynthesis of this sesquiterpene. On the other hand, the peak enrichment of five carbons of ¹³C-artemisinin including carbon atoms originating from methyls of dimethylallyl group of geranyl pyrophosphate (GPP) and farnesyl pyrophosphate (FPP) was observed from [1,6-¹³C₂]glucose. This suggested that GPP which is supposed to be biosynthesized in plastids travels from plastids to cytosol through the plastidial wall and combines with isopentenyl pyrophosphate (IPP) to form the (E,E)-FPP which finally cyclizes and oxidizes to artemisinin. In this way the DXP pathway also contributes to the biosynthesis of this sesquiterpene.     

Influence of enhanced CO2 on growth and photosynthesis of the red algaeGracilaria sp. andG. chilensis

The influence of elevated CO₂ concentrations on growth and photosynthesis ofGracilaria sp. andG. chilensis was investigated in order to procure information on the effective utilization of CO₂. Growth of both was enhanced by CO₂ enrichment (air + 650 ppm CO₂, air + 1250 ppm CO₂, the enhancement being greater inGracilaria sp. Both species increased uptake of NO₃ ^– with CO₂ enrichment. Photosynthetic inorganic carbon uptake was depressed inG. chilensis by pre-culture (15 days) with CO₂ enrichment, but little affected inGracilaria sp. Mass spectrometric analysis showed that O₂ uptake was higher in the light than in the dark for both species and in both cases was higher inGracilaria sp. The higher growth enhancement inGracilaria sp. was attributed to greater depression of photorespiration by the enrichment of CO₂ in culture.     

C4 photosynthetic carbon metabolism in the leaves of aromatic tropical grasses — I. Leaf anatomy,CO2 compensation point and CO2 assimilation

A few species of Cymbopogon and Vetiveria are potentially important tropical grasses producing essential oils. In the present study, we report on the leaf anatomy and photosynthetic carbon assimilation in five species of Cymbopogon and Vetiveria zizanioides. Kranz-type leaf anatomy with a centrifugal distribution of chloroplasts and exclusive localization of starch in the bundle sheath cells were common among the test plants. Besides the Kranz leaf anatomy, these grasses displayed other typical C₄ characteristics including a low (0–5 µl/l) CO₂ compensation point, lack of light saturation of CO₂ uptake at high photon flux densities, high temperature (35°C) optimum of net photosynthesis, high rates of net photosynthesis (55–67 mg CO₂ dm^-2 leaf area h^-1), little or no response of net photosynthesis to atmospheric levels of O₂ and high leaf ¹³C/¹²C ratios. The biochemical studies with ¹⁴CO₂ indicated that the leaves of the above plant species synthesize predominantly malate during short term (5 s) photosynthesis. In pulse-chase experiments it was shown that the synthesis of 3-phosphoglycerate proceeds at the expense of malate, the major first formed product of photosynthesis in these plant species.     

Allocation of carbon to shoots,roots, soil and rhizosphere respiration by barrel medic (Medicago truncatula) before and after defoliation

The allocation of carbon to shoots, roots, soil and rhizosphere respiration in barrel medic (Medicago truncatulaGaertn.) before and after defoliation was determined by growing plants in pots in a labelled atmosphere in a growth cabinet. Plants were grown in a ¹⁴CO₂-labelled atmosphere for 30 days, defoliated and then grown in a ¹³CO₂-labelled atmosphere for 19 days. Allocation of ¹⁴C-labelled C to shoots, roots, soil and rhizosphere respiration was determined before defoliation and the allocation of ¹⁴C and ¹³C was determined for the period after defoliation. Before defoliation, 38.4% of assimilated C was allocated below ground, whereas after defoliation it was 19.9%. Over the entire length of the experiment, the proportion of net assimilated carbon allocated below ground was 30.3%. Of this, 46% was found in the roots, 22% in the soil and 32% was recovered as rhizosphere respiration. There was no net translocation of assimilate from roots to new shoot tissue after defoliation, indicating that all new shoot growth arose from above-ground stores and newly assimilated carbon. The rate of rhizosphere respiration decreased immediately after defoliation, but after 8 days, was at comparable levels to those before defoliation. It was not until 14 days after defoliation that the amount of respiration from newly assimilated C (¹³C) exceeded that of C assimilated before defoliation (¹⁴C). This revised version was published online in June 2006 with corrections to the Cover Date.     

Elevated [CO2], temperature increase and N supply effects on the turnover of below-ground carbon in a temperate grassland ecosystem

The effects of elevated [CO₂] (700 μl l^-1 CO₂) and temperature increase (+3 °C) on carbon turnover in grassland soils were studied during 2.5 years at two N fertiliser supplies (160 and 530 kg N ha^-1 y^-1) in an experiment with well-established ryegrass swards (Lolium perenne) supplied with the same amounts of irrigation water. During the growing season, swards from the control climate (350 μl l^-1 [CO₂] at outdoor air temperature) were pulse labelled by the addition of ¹³CO₂. The elevated [CO₂] treatments were continuously labelled by the addition of fossil-fuel derived CO₂ (^{13 C} of -40 to -50 ‰). Prior to the start of the experimental treatments, the carbon accumulated in the plant parts and in the soil macro-organic matter (‘old’ C) was at −32‰. During the experiment, the carbon fixed in the plant material (‘new’ C) was at −14 and −54‰ in the ambient and elevated [CO₂] treatments, respectively. During the experiment, the ¹³C isotopic mass balance method was used to calculate, for the top soil (0–15 cm), the carbon turnover in the stubble and roots and in the soil macro-organic matter above 200 μ (MOM). Elevated [CO₂] stimulated the turnover of organic carbon in the roots and stubble and in the MOM at N+, but not at N−. At the high N supply, the mean replacement time of ‘old’ C by ‘new’ C declined in elevated, compared to ambient [CO₂], from 18 to 7 months for the roots and stubble and from 25 to 17 months for the MOM. This resulted from increased rates of ‘new’ C accumulation and of ‘old’ C decay. By contrast, at the low N supply, despite an increase in the rate of accumulation of ‘new’ C, the soil C pools did not turnover faster in elevated [CO₂], as the rate of ‘old’ C decomposition was reduced. A 3 °C temperature increase in elevated [CO₂] decreased the input of fresh C to the roots and stubble and enhanced significantly the exponential rate for the ‘old’ C decomposition in the roots and stubble. An increased fertiliser N supply reduced the carbon turnover in the roots and stubble and in the MOM, in ambient but not in elevated [CO₂]. The respective roles for carbon turnover in the coarse soil OM fractions, of the C:N ratio of the litter, of the inorganic N availability and of a possible priming effect between C-substrates are discussed. This revised version was published online in June 2006 with corrections to the Cover Date.     

A pulse-labelling method to generate 13C- enriched plant materials

Plant materials labelled with ¹³C can be used to trace litter decomposition and root carbon flow, but only if the isotope is uniformly distributed in the plant. We postulated that if ¹³CO₂ were applied at regular intervals, in direct proportion to the rate of photosynthesis, then the abundance of ¹³C would be uniform among plant parts. To test this hypothesis, wheat plants were grown in the greenhouse, and exposed weekly to ¹³CO₂ for six hours in a closed chamber. A constant dose of ¹³CO₂ (about 33 atom%) was injected whenever CO₂ concentration fell below a prescribed limit, so that ¹³CO₂ was added in proportion to photosynthetic rate. Wheat exposed for 13 weeks (starting 11 days after seeding) had reasonably consistent ¹³C abundance among plant parts: grain = 3.41, chaff = 3.41, stem = 3.65, and root = 3.50 atom%. The `leaf' fraction had slightly higher abundance (3.99 atom%), perhaps because recently-fixed ¹³C was not translocated from senescing tissue. Exposing plants only during early stages of the growing season increased differences among plant parts. The approach offers a practical way to label plants with ¹³C.     

Carbon isotope composition of intermediates of the starch-malate sequence and level of the crassulacean acid metabolism in leaves of Kalanchoe blossfeldiana Tom Thumb

Isotype analyses were performed on biochemical fractions isolated from leaves of Kalanchoe blossfeldiana Tom Thumb. during aging under long days or short days. Irrespective of the age or photoperiodic conditions, the intermediates of the starch-malate sequence (starch, phosphorylated compounds and organic acids) have a level of ¹³C higher than that of soluble sugars, cellulose and hemicellulose. In short days, the activity of the crassulacean acid metabolism pathway is predominant as compared to that of C₃ pathway: leaves accumulate organic acids, rich in ¹³C. In long days, the activity of the crassulacean acid metabolism pathway increases as the leaves age, remaining, however, relatively low as compared to that of C₃ pathway: leaves accumulate soluble sugars, poor in ¹³C. After photoperiodic change (long daysshort days), isotopic modifications of starch and organic acids suggest evidence for a lag phase in the establishment of the crassulacean acid metabolism pathway specific to short days. The relative proportions of carbon from a C₃-origin (RuBPC acitivity as strong discriminating step, isotope discrimination in vivo=20) or C₄-origin (PEPC activity as weak discriminating step, isotope discrimination in vivo=4) present in the biochemical fractions were calculated from their ¹³C values. Under long days, 30 to 70% versus 80 to 100% under short days, of the carbon of the intermediates linked to the starch-malate sequence, or CAM pathway (starch, phosphorylated compounds and organic acids), have a C₄-origin. Products connected to the C₃ pathway (free sugars, cellulose, hemicellulose) have 0 to 50% of their carbon, arising from reuptake of the C₄ from malate, under long days versus 30 to 70% under short days.Abbreviations CAM crassulacean acid metabolism - CAM pathway pathway with malate accumulation by -carboxylation of PEP, arising from glycolysis of starch (starch-malate sequence) - C₃-metabolism metabolism with primary carbon fixed by the Calvin and Benson pathway (C₃-origin) - C₄-metabolism metabolism with primary carbon fixed by the Hatch and Slack pathway (C₄-origin) - C₃-pathway pathway with RuBPC activity and the Calvin and Benson pathway, irrespective of the CO₂-source, atmospheric or reuptake of the C₄ from malate - ¹³C()=(R_sample-R_PDR)10³/R_PDB where PDB Pee Dee belemnite (belemnite from the Pee Dee formation, South Carolina) and R=¹³C/¹²C - D isotope discrimination - PEP phosphoenolpyruvate - PEPC (EC 4.1.1.31) PEP carboxylase - PGA phosphoglyceric acid - Py.di-PK (EC 2.7.9.1) pyruvate, Pi-dikinase - RuBP ribulose bisphosphate - RuBPC (EC 4.1.1.39) RuBP carboxylase - SD short days - LD long days     

δ<Superscript>13</Superscript>C values,photosynthetic pathways,and plant functional types for some plants from saline meadows,Northeastern China

Based on stable carbon isotope ratio (δ¹³C) measurements, photosynthetic pathway types were determined for 61 species in 54 genera and 24 families of flowering plants from the saline meadows of Northeastern China. Of these total vascular plants, 18 species in 17 genera from 6 families were found to have C₄ photosynthesis; 43 species in 38 genera from 20 families had C₃ photosynthesis. Six dicotyledonous species exhibited C₄ pathway, 12 monocotyledonous species were found with C₄ photosynthesis. The dicotyledonous C₄ species had relative greater mean δ¹³C value and less total carbon content than both monocotyledonous C₄ and C₃ species. Most dicotyledonous C₄ species were annual forbs and halophytes. Some C₄ species had been previously documented, but their δ¹³C values varied remarkably from those of the present study. Even though there are some fluctuations for the δ¹³C values of some C₄ species, δ¹³C value was still more reliable for C₃ and C₄ identification than the use of the enzyme ratio method and of low CO₂ compensation concentration.     

Two distinct plant respiratory physiotypes might exist which correspond to fast-growing and slow-growing species

The origin of the carbon atoms in CO₂ respired by leaves in the dark of several plant species has been studied using ¹³C/¹²C stable isotopes. This study was conducted using an open gas exchange system for isotope labeling that was coupled to an elemental analyzer and further linked to an isotope ratio mass spectrometer (EA–IRMS) or coupled to a gas chromatography–combustion-isotope ratio mass spectrometer (GC–C-IRMS). We demonstrate here that the carbon, which is recently assimilated during photosynthesis, accounts for nearly ca. 50% of the carbon in the CO₂ lost through dark respiration (R_d) after illumination in fast-growing and cultivated plants and trees and, accounts for only ca. 10% in slow-growing plants. Moreover, our study shows that fast-growing plants, which had the largest percentages of newly fixed carbon of leaf-respired CO₂, were also those with the largest shoot/root ratios, whereas slow-growing plants showed the lowest shoot/root values.     

Carbon isotopes and carbon turnover in cotton and wheat FACE experiments

The Maricopa cotton and wheat FACE (free-air CO₂ enrichment) experiments offer propitious opportunity to quantify carbon turnover. The commercial CO₂ (% MathType!MTEF!2!1!+-% feaafiart1ev1aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn% hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr% 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq-Jc9% vqaqpepm0xbba9pwe9Q8fs0-yqaqpepae9pg0FirpepeKkFr0xfr-x% fr-xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaGaeqiTdq2aaW% baaSqabeaacaaIXaGaaG4maaaakiaaboeacqGHijYUcqGHsislcaaI% ZaGaaG4naiaacwcaliaad+gaaaa!3FCB!\[\delta ^{13} {\text{C}} \approx - 37\% o\]) used to elevate CO₂ concentration in field plots provided a strongly ¹³C-depleted tracer. Soil CO₂ and ¹³C of soil organic carbon (SOC) in CO₂-enriched and Control plots were measured between the final cotton FACE project (October 1991) and the end of the second wheat experiment (June 1994). The initial ¹³C-depletion in SOC of cotton FACE plots (measured by the difference in ¹³C between FACE and Control plots) persisted at the same level (1.9) 1.5 years after the experiment ended. A similar depletion was observed in soil CO₂ evolved in the same plots, indicating ongoing decomposition of the new SOC. The SOC ¹³C of wheat plots before and after two growing seasons showed increasing ¹³C-depletion in FACE relative to Control. Isotopic mass balance was consistent with 5–6% new carbon input from the two wheat crops. This is lower than the 12–13% calculated for FACE cotton and perhaps a consequence of the larger root system of cotton or the 3-year duration of the cotton experiments versus 2 years for the wheat.     

C4 photosynthesis in Spartina townsendii at low and high temperatures

The metabolism of ¹⁴CO₂ in the cool temperate saltmarsh grass Spartina townsendii was investigated in plants grown in their natural habitats at two temperatures. Both in the spring at 10°C and in the late summer at 25°C radioactivity was initially incorporated into the organic acids malate and aspartate and then transferred to 3-phosphoglycerate in the manner characteristic of the C₄ pathway of photosynthesis. Metabolism was not disrupted at the lower temperature as in some C₄ plants. Radioactivity was transferred more slowly from malate into alanine, glycine and serine at 10°C, but sugars were labelled equally at both temperatures.